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Stable oxygen isotopic records in ice cores provide valuableinformation about past temperature, especially for regions with scarceinstrumental measurements. This paper presents the δ18O resultof an ice core drilled to bedrock from Mt. Zangser Kangri (ZK), a remotearea on the northern Tibetan Plateau (TP). We reconstructed the temperatureseries for 1951–2008 from the δ18O records. In addition, wecombined the ZK δ18O records with those from three other icecores in the northern TP (Muztagata, Puruogangri, and Geladaindong) toreconstruct a regional temperature history for the period 1951–2002 (RTNTP).The RTNTP showed significant warming at 0.51 ± 0.07 °C(10 yr)−1 since 1970, a higher rate than the trend of instrumentalrecords of the northern TP (0.43 ± 0.08 °C (10 yr)−1) andthe global temperature trend (0.27 ± 0.03°C (10 yr)−1) atthe same time. In addition, the ZK temperature record, with extra lengthuntil 2008, seems to suggest that the rapid elevation-dependent warmingcontinued for this region during the last decade, when the mean globaltemperature showed very little change. This could provide insights into thebehavior of the recent warming hiatus at higher elevations, whereinstrumental climate records are lacking

climate of the past

Significant recent warming over the northern Tibetan Plateau from ice core &amp;lt;i&amp;gt;δ&amp;lt;/i&amp;gt;&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O records